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dc.contributor.author | Balasch, Josep Carles | es_ES |
dc.contributor.author | Calvet, Jaume | es_ES |
dc.contributor.author | Tuset, Jordi | es_ES |
dc.coverage.spatial | east=0.5287362; north=40.5541008; name=Les Cases d'Alcanar, Tarragona, Espanya | es_ES |
dc.date.accessioned | 2023-02-08T08:13:16Z | |
dc.date.available | 2023-02-08T08:13:16Z | |
dc.date.issued | 2023-01-31 | |
dc.identifier.issn | 1134-2196 | |
dc.identifier.uri | http://hdl.handle.net/10251/191705 | |
dc.description.abstract | [EN] The paper studies the flash-flood that took place on September the 1st, 2021 in Les Cases d'Alcanar (Tarragona). Its meteorological and hydrological characteristics make it one of the most remarkable on the Western Mediterranean coast. A post-event reconstruction was carried out, which involved the determination of the peak flow using the 2D IBER hydraulic model and the hydrological response of the basin applying the HEC-HMS lumped model software. After a rain depth of 251.9 mm in 3 hours, the peak flow reached 159 m3·s-1 in the town and the runoff volume was 1.15 hm3. The runoff coefficient was 0.76. A large part of the overflow in the urban area was due to the occlusion of the transversal drainages structures. The reconstructed data will be of great value for the planning of structures in small basins that generally lack data from gage stations. | es_ES |
dc.description.abstract | [ES] La crecida que se produjo el 1 de septiembre de 2021 en Les Cases d Alcanar (Tarragona), es una de las de mayor magnitud del litoral mediterráneo occidental durante la época instrumental. Se ha realizado una reconstrucción post-evento determinando el caudal punta mediante el modelo hidráulico 2D IBER y la respuesta hidrológica de la cuenca a través del software hidrológico global HEC-HMS. Tras una lluvia de 251,9 mm en unas 3 horas, se estima que el pico fue de 159 m3·s-1 a la entrada de la población y el volumen de escorrentía fue de 1,15 hm3. El coeficiente de escorrentía alcanzó a 0,76. Gran parte del desbordamiento en el núcleo poblado fue debido a la oclusión de los drenajes transversales al torrente y a la falta de capacidad de drenaje del canal. Los datos reconstruidos se consideran de un gran valor para la planificación de estructuras en cuencas pequeñas que carecen de datos de aforo. | es_ES |
dc.language | Español | es_ES |
dc.publisher | Universitat Politècnica de València | es_ES |
dc.relation.ispartof | Ingeniería del Agua | es_ES |
dc.rights | Reconocimiento - No comercial - Compartir igual (by-nc-sa) | es_ES |
dc.subject | Flash-flood | es_ES |
dc.subject | Hydraulic reconstruction | es_ES |
dc.subject | Hydrological modelling | es_ES |
dc.subject | Montsià Range | es_ES |
dc.subject | Inundación súbita | es_ES |
dc.subject | Reconstrucción hidráulica | es_ES |
dc.subject | Modelización hidrológica | es_ES |
dc.subject | Serra de Montsià | es_ES |
dc.title | Reconstrucción post-evento del flash-flood del 1 de septiembre de 2021 en Les Cases d' Alcanar (Tarragona) | es_ES |
dc.title.alternative | Post-event survey and reconstruction of the September 2021 flash-flood in Les Cases d' Alcanar (Tarragona) | es_ES |
dc.type | Artículo | es_ES |
dc.identifier.doi | 10.4995/ia.2023.18535 | |
dc.rights.accessRights | Abierto | es_ES |
dc.description.bibliographicCitation | Balasch, JC.; Calvet, J.; Tuset, J. (2023). Reconstrucción post-evento del flash-flood del 1 de septiembre de 2021 en Les Cases d' Alcanar (Tarragona). Ingeniería del Agua. 27(1):29-44. https://doi.org/10.4995/ia.2023.18535 | es_ES |
dc.description.accrualMethod | OJS | es_ES |
dc.relation.publisherversion | https://doi.org/10.4995/ia.2023.18535 | es_ES |
dc.description.upvformatpinicio | 29 | es_ES |
dc.description.upvformatpfin | 44 | es_ES |
dc.type.version | info:eu-repo/semantics/publishedVersion | es_ES |
dc.description.volume | 27 | es_ES |
dc.description.issue | 1 | es_ES |
dc.identifier.eissn | 1886-4996 | |
dc.relation.pasarela | OJS\18535 | es_ES |
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